Reaction‐Induced Mantle Weakening at High‐Pressure Conditions: An Example From Garnet Pyroxenites of Ulten Zone (Eastern Alps, N Italy)-Reference-Cited by-同舟云学术

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Reaction‐Induced Mantle Weakening at High‐Pressure Conditions: An Example From Garnet Pyroxenites of Ulten Zone (Eastern Alps, N Italy)

Published:2021-12 Issue:12 Volume:126 Page:
ISSN:2169-9313
Container-title:Journal of Geophysical Research: Solid Earth
language:en
Short-container-title:JGR Solid Earth

Author:

Pellegrino L.¹^ORCID,Menegon L.²^ORCID,Zanchetta S.¹^ORCID,Langenhorst F.³⁴,Pollok K.³^ORCID,Tumiati S.⁵^ORCID,Malaspina N.¹

Affiliation:

1. Department of Earth and Environmental Sciences University of Milano‐Bicocca Milano Italy

2. Department of Geosciences The Njord Centre University of Oslo Oslo Norway

3. Institute of Geosciences Friedrich Schiller University Jena Jena Germany

4. School of Ocean and Earth Science and Technology Hawai’i Institute of Geophysics and Planetology University of Hawai’i at Manoa Honolulu USA

5. Department of Earth Sciences University of Milano Milano Italy

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2021JB022584

Reference135 articles.

1. An experimental study of two garnet pyroxenite xenoliths from the Bullenmerri and Gnotuk Maars of western Victoria, Australia

2. Implications of a two-component marble-cake mantle

3. Diffusion-accommodated flow and superplasticity

4. Texture Analysis with MTEX – Free and Open Source Software Toolbox

5. High-temperature creep of olivine single crystals III. Mechanical results for unbuffered samples and creep mechanisms

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